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TRAVEL Hubbard Glacier AlaskA CRUISE PHOTOS
Hubbard Glacier is a tidewater glacier in the U.S. state of Alaska and the
Yukon Territory of Canada. From its source in the Yukon, the glacier
stretches 122 km (76 mi) to the sea at Yakutat Bay and Disenchantment Bay.
It is the longest tidewater glacier in Alaska, with an open calving face
over ten kilometers (6 mi) wide.

Hubbard Glacier’s longest source, 122 km from its snout, is at about 11,000
feet above sea level at about 61-00N 140-09 W, about eight kilometers west
of Mt. Walsh. A shorter tributary glacier begins at the easternmost summit
on the Mt. Logan ridge at about 18,300 feet at about 60-35 N 140-22-40 W.

Before it reaches the sea, Hubbard is joined by the Valerie Glacier to the
west, which, through forward surges of its own ice, has contributed to the
advance of the ice flow that experts believe will eventually dam the Russell
Fiord from Disenchantment Bay waters.

The Hubbard Glacier ice margin has continued to advance for about a century.
In May 1986, the Hubbard Glacier surged forward, blocking the outlet of
Russell Fiord and creating "Russell Lake." All that summer the new lake
filled with runoff; its water level rose 25 meters, and the decrease in
salinity threatened its sea life.

Around midnight on October 8 the dam began to give way. In the next 24 hours
an estimated 5.3 km³ of water gushed through the gap, and the fiord was
reconnected to the ocean at its previous level. This was the second largest
glacial lake outburst flood (GLOF) in recorded history.

In spring 2002, the glacier again approached Gilbert Point. It pushed a
terminal moraine ahead of its face and closed the opening again in July. On
August 14, the terminal moraine was washed away after rains had raised the
water level behind the dam it formed to 18 m (61 ft) above sea level.
The fiord could become dammed again, and perhaps permanently. If this
happens, the fiord could overflow its southern banks and drain through the
Situk River instead, threatening trout habitat and a local airport.
The ice at the foot of Hubbard Glacier is about 400 years old: it takes that
long for ice to traverse the length of the glacier. The glacier routinely
calves off icebergs the size of a ten-story building. Where the glacier
meets the shore, most of the ice is below the waterline, and newly calved
icebergs can shoot up quite dramatically, so that ships must keep their
distance from it as they ply their way up and down the coast.
submitted by Willie Shoemaker (Fabens, Texas)
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